“…In some places of the CIZ, the lower crust was significantly thinned by pervasive extension and widespread melting processes (Alcock et al., 2015; Ayarza et al., 2021; Díez Fernández & Pereira, 2016; Escuder Viruete et al., 1998; Martínez Catalán et al., 2014), also evidenced by the intrusion of late‐Variscan granitoids (e.g., Bea et al., 2003; Orejana et al., 2012; Simancas et al., 2013). The generalized gravitational collapse of this orogen and crustal thinning was driven by broad ductile shear zones that formed under a regional N‐S to NW‐SE direction of extension (e.g., Dias da Silva et al., 2021; Doblas, 1991; Doblas, López‐Ruiz, et al., 1994; Escuder Viruete et al., 1998). Associated to these late‐Variscan low‐angle detachment tectonics and shear zones, uplift of deep and hot rocks in the footwall of these detachments caused a progressive doming of the overlying mylonitic zone resulting in an asymmetric antiform (Doblas, López‐Ruiz, et al., 1994; Escuder Viruete et al., 1994).…”